摘要
本文从宏观(结构、构造、接触关系)微观(岩石化学、微量元素、稀土元素、副矿物)对比出发,按国际地层指南的将课成岩体“属于地层学和地层划分的范畴”的思路,将管店岩体划分成石马凹单元、南封单元、小寺王单元和祝刘单元四个单元,合并成管店超单元。并对岩浆受构造应力驱使由南向北挤侵就位证据进行了探讨。
This paper discussed texture.structure .contact; relationship, chemical compositions, microelements, REE and mineral assemblages, etc, of the Guandian granite body. Based on abrief of pedigree method, Guandian granite body can be divided into four lithodemic unites:Nanfeng unite,shima'ao unite, Xiaosiwang unite and Zhuliu unite. The paper also discussedthe evidence of the squeezing emplacement of the magma driven by tectonic stress.
出处
《火山地质与矿产》
1995年第4期37-44,共8页
Volcanology & Mineral Resources
关键词
岩石谱系单位
岩浆
就位机制
管店岩体
岩石
lithodemic unite, emplacing mechanism of the granite magma, Guandian granite body